Regions
Kootenay Boundary.
The heat is on and the game is changing. The strong spring sun and increasingly warm temperatures are expected to further destabilize the upper 20 to 30 cm of snow and a natural avalanche cycle is very likely. Even deeper avalanches are possible.
Weather Forecast
Hot days & warm nights look to be with us through at least Thursday. Say goodbye to any kind of temperature driven overnight re-freeze for the next few days. This weather event is having a pretty significant impact on our snowpack.SUNDAY NIGHT: Clear skies, light northerly wind, freezing level rising to around 2500 m, no precipitation, no overnight re-freeze.MONDAY: Clear skies, light variable wind, freezing level holding at 2500 m, no precipitation, no overnight re-freeze.TUESDAY: Clear skies, light southeast wind, freezing level fixed at 2800 m, no precipitation, no overnight re-freeze.WEDNESDAY: Clear skies, moderate southeast wind, freezing level fixed at 2800 m, no precipitation, no overnight re-freeze.
Avalanche Summary
Saturday (which was colder and cloudier than Sunday) initiated a natural avalanche cycle that featured loose moist avalanches to size 2.5 on south and southeast facing slopes between 1400 and 1600 m as the old storm snow slid on a crust before stepping down to basal (deep) weak layers.On Friday a couple of small wind and storm slabs were reported on northeast, east and south facing slopes. These avalanches were failing on the facet/crust combo just under the most recent snow, this activity likely picked up on Sunday and is expected to be even more active on Monday.
Snowpack Summary
Solar aspects (south and west) were sporting a new crust Saturday. Sunday's blast of heat has likely eliminated any trace of cold snow, but you may still find some on high elevation north features. Wind slabs are likely done at this point, zapped of their strength by time and warming.We're not expecting any overnight re-freeze Sunday night, and we're very concerned about the upper 20 to 30 cm of snow that sits on a mix of facets and crust.The bigger questions are deeper in the snowpack. We have at least three prominent weak layers in the upper meter and we're not expecting an overnight re-freeze for the foreseeable future. That's going to allow the snowpack to warm which starts freeing up a lot of water which lubricates the upper snowpack. It also allows the upper snowpack to start creeping downhill at an accelerated rate. When it doesn't freeze overnight, this process gets turbo-charged. How many hot days and warm nights will it take to wake up the more deeply buried weak layers? We're not sure, but now is probably a time to let the mountains do their thing from afar and check back in when the freezing level returns to seasonal norms which could happen by next weekend.
Problems
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.
Loose Wet
Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.